Geochemistry of the Triassic to Jurassic plutonism of central Chile (30 to 33°S); petrogenetic implications and a tectonic discussion

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Artículo de libro Serie Special Paper. Geological Society of America, n.265.Editor: Boulder, CO: Geological Society of America, 1991Descripción: pp. 99-112 ilus., map., tbls.Tema(s): GEOQUÍMICA

Tipo de ítem	Ubicación actual	Colección	Signatura	Estado	Fecha de vencimiento	Código de barras
Artículo de libro	Biblioteca INGEMMET	Colección Digital	552.11(238.1)/H22\|3 (Navegar estantería)	Disponible		14326
Libro	Biblioteca INGEMMET		552.11(238.1)/H22 (Navegar estantería)	Disponible		2241

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Previo	552.11(238.1)/H22\|19 The source of central Andean magmas; some considerations	552.11(238.1)/H22\|2 Geochemical features of southern Andes Quaternary volcanics between 41°50' and 43°00'S	552.11(238.1)/H22\|20 Triassic rifting and associated basalts in the Cuyo basin, central Argentina	552.11(238.1)/H22\|3 Geochemistry of the Triassic to Jurassic plutonism of central Chile (30 to 33°S); petrogenetic implications and a tectonic discussion	552.11(238.1)/H22\|4 Magma source variations for mid-late Tertiary magmatic rocks associated with a shallowing subduction zone and a thickening crust in the Central Andes (28 to 33°S)	552.11(238.1)/H22\|5 On the isostatic state of the eastern Alps and the Central Andes; a statistical comparison	552.11(238.1)/H22\|7 Petrologic and tectonic evolution of the Cenozoic volcanism in the Bolivian western Andes	Siguiente

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Previo								Siguiente
Previo	552.11(238.1)/H22\|19 The source of central Andean magmas; some considerations	552.11(238.1)/H22\|2 Geochemical features of southern Andes Quaternary volcanics between 41°50' and 43°00'S	552.11(238.1)/H22\|20 Triassic rifting and associated basalts in the Cuyo basin, central Argentina	552.11(238.1)/H22\|3 Geochemistry of the Triassic to Jurassic plutonism of central Chile (30 to 33°S); petrogenetic implications and a tectonic discussion	552.11(238.1)/H22\|4 Magma source variations for mid-late Tertiary magmatic rocks associated with a shallowing subduction zone and a thickening crust in the Central Andes (28 to 33°S)	552.11(238.1)/H22\|5 On the isostatic state of the eastern Alps and the Central Andes; a statistical comparison	552.11(238.1)/H22\|7 Petrologic and tectonic evolution of the Cenozoic volcanism in the Bolivian western Andes	Siguiente

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